Journal of Himalayan Geology, Volumes 1-2Wada Institute of Himalayan Geology, 1990 - Geology |
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Page 133
showing variations across the chain in the speed with which rock moves upward ,
away from the centre of the earth ( Molnar , 1987c ) . or Seismicity and Fault
Plane Solutions Most well located earthquakes in the Himalaya have occurred ...
showing variations across the chain in the speed with which rock moves upward ,
away from the centre of the earth ( Molnar , 1987c ) . or Seismicity and Fault
Plane Solutions Most well located earthquakes in the Himalaya have occurred ...
Page 134
Map showing epicentres and fault plane solutions of moderate earthquakes since
1963 ( Table 1 ) , epicentres of major earthquakes ( M > 7 ) since 1900 , and
rupture zones of great earthquakes ( M > 8 ) since 1897. In lower hemisphere ...
Map showing epicentres and fault plane solutions of moderate earthquakes since
1963 ( Table 1 ) , epicentres of major earthquakes ( M > 7 ) since 1900 , and
rupture zones of great earthquakes ( M > 8 ) since 1897. In lower hemisphere ...
Page 137
The solutions for one event ( 15 August , 66 ) indicates normal faulting with a T -
axis approximately perpendicular to the chain , and that for a less well
constrained solution ( 19 June , 79 ) appears to be similar ( Fig . 2 , Table 1 ) .
These events ...
The solutions for one event ( 15 August , 66 ) indicates normal faulting with a T -
axis approximately perpendicular to the chain , and that for a less well
constrained solution ( 19 June , 79 ) appears to be similar ( Fig . 2 , Table 1 ) .
These events ...
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Contents
The Shyok valley Northern Ladakh India An entraped and compressed marginal | 1 |
Chemical mineralogy of the Panjal Traps around Bandipura Kashmir | 17 |
Structural characteristics of the rocks of BanihalRamban area | 23 |
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activity associated authors basin beds belt biotite block Central correlation Crystallines deformation deposits developed District dolerite earthquakes eastern et al event exposed extends facies fault feldspars field folds followed Formation formed Garhwal Geol Geology gneisses grade grains granite granitoids Group higher Himalaya Himalayan Geology hornblende India indicate Indus Institute Jour Krol Ladakh Late later Lesser Himalaya limestone lower Main major margin material metamorphism Middle minerals nature Nayar northern observed occur oceanic ophiolitic origin phase phyllite plagioclase plane plate Pradesh present quartz quartzite range References region represented result river rocks Salt samples sandstone schist sedimentary sediments sequence Series shale Sharma Shyok Siwalik slip slope southern Spiti structural Subathu subduction suggests surface Suture Table tectonic thick Thrust trend units Upper valley values variation volcanics Wadia western zone